Late Quaternary high-temperature geyserites in the Ol’khon area, Baikal rift zone: Petrography, mineralogy, chemical composition, and genesis

Abstract Late Quaternary geyserites in the Ol’khon area, Baikal rift zone, are a geologically and petrologically unique rocks, which may provide information on the character of hydrothermal processes during the development of modern rift zones. The geyserites of this area are characterized by the pr...
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Autor*in:	Sklyarov, E. V. [verfasserIn] Skovitina, T. M. Sklyarova, O. A. Kotov, A. B. Tolmacheva, E. V. Velikoslavinskii, S. D.

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2014

Schlagwörter:	Travertine Rift Zone Siberian Craton Siliceous Material Chalcedony

Anmerkung:	© Pleiades Publishing, Ltd. 2014

Übergeordnetes Werk:	Enthalten in: Petrology - Moscow : MAIK Nauka/Interperiodica Publ. [u.a.], 1996, 22(2014), 6 vom: Nov., Seite 536-546
Übergeordnetes Werk:	volume:22 ; year:2014 ; number:6 ; month:11 ; pages:536-546

Links:	Volltext

DOI / URN:	10.1134/S0869591114060046

Katalog-ID:	SPR020203357

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245	1	0	\|a Late Quaternary high-temperature geyserites in the Ol’khon area, Baikal rift zone: Petrography, mineralogy, chemical composition, and genesis
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520			\|a Abstract Late Quaternary geyserites in the Ol’khon area, Baikal rift zone, are a geologically and petrologically unique rocks, which may provide information on the character of hydrothermal processes during the development of modern rift zones. The geyserites of this area are characterized by the presence of minerals atypical of such rocks: highly crystalline graphite (which is usually formed at high temperatures) and α-carbyne (which is a natural carbon modification that has been previously found only among products of experiments). Other newly formed minerals of the geyserites are equilibrium chalcedony, talc, and tremolite. This suggests that the rocks were formed under conditions significantly different from those under which classic geyserites are produced. Geyserites in the Ol’khon area were most probably produced by silica-saturated solutions rich in certain ore components (Fe, Mn, Sb, As, and Y) and heated to temperatures of about 400°C.
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700	1		\|a Skovitina, T. M. \|4 aut
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700	1		\|a Kotov, A. B. \|4 aut
700	1		\|a Tolmacheva, E. V. \|4 aut
700	1		\|a Velikoslavinskii, S. D. \|4 aut
773	0	8	\|i Enthalten in \|t Petrology \|d Moscow : MAIK Nauka/Interperiodica Publ. [u.a.], 1996 \|g 22(2014), 6 vom: Nov., Seite 536-546 \|w (DE-627)511882602 \|w (DE-600)2235750-6 \|x 1556-2085 \|7 nnns
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912			\|a GBV_ILN_151
912			\|a GBV_ILN_152
912			\|a GBV_ILN_161
912			\|a GBV_ILN_170
912			\|a GBV_ILN_171
912			\|a GBV_ILN_187
912			\|a GBV_ILN_213
912			\|a GBV_ILN_224
912			\|a GBV_ILN_230
912			\|a GBV_ILN_250
912			\|a GBV_ILN_281
912			\|a GBV_ILN_285
912			\|a GBV_ILN_293
912			\|a GBV_ILN_370
912			\|a GBV_ILN_602
912			\|a GBV_ILN_636
912			\|a GBV_ILN_702
912			\|a GBV_ILN_2001
912			\|a GBV_ILN_2003
912			\|a GBV_ILN_2004
912			\|a GBV_ILN_2005
912			\|a GBV_ILN_2006
912			\|a GBV_ILN_2007
912			\|a GBV_ILN_2008
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912			\|a GBV_ILN_2031
912			\|a GBV_ILN_2034
912			\|a GBV_ILN_2037
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912			\|a GBV_ILN_2044
912			\|a GBV_ILN_2048
912			\|a GBV_ILN_2049
912			\|a GBV_ILN_2050
912			\|a GBV_ILN_2055
912			\|a GBV_ILN_2057
912			\|a GBV_ILN_2059
912			\|a GBV_ILN_2061
912			\|a GBV_ILN_2064
912			\|a GBV_ILN_2065
912			\|a GBV_ILN_2068
912			\|a GBV_ILN_2070
912			\|a GBV_ILN_2086
912			\|a GBV_ILN_2088
912			\|a GBV_ILN_2093
912			\|a GBV_ILN_2106
912			\|a GBV_ILN_2107
912			\|a GBV_ILN_2108
912			\|a GBV_ILN_2110
912			\|a GBV_ILN_2111
912			\|a GBV_ILN_2112
912			\|a GBV_ILN_2113
912			\|a GBV_ILN_2116
912			\|a GBV_ILN_2118
912			\|a GBV_ILN_2119
912			\|a GBV_ILN_2122
912			\|a GBV_ILN_2129
912			\|a GBV_ILN_2143
912			\|a GBV_ILN_2144
912			\|a GBV_ILN_2147
912			\|a GBV_ILN_2148
912			\|a GBV_ILN_2152
912			\|a GBV_ILN_2153
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912			\|a GBV_ILN_4037
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allfields	10.1134/S0869591114060046 doi (DE-627)SPR020203357 (SPR)S0869591114060046-e DE-627 ger DE-627 rakwb eng Sklyarov, E. V. verfasserin aut Late Quaternary high-temperature geyserites in the Ol’khon area, Baikal rift zone: Petrography, mineralogy, chemical composition, and genesis 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2014 Abstract Late Quaternary geyserites in the Ol’khon area, Baikal rift zone, are a geologically and petrologically unique rocks, which may provide information on the character of hydrothermal processes during the development of modern rift zones. The geyserites of this area are characterized by the presence of minerals atypical of such rocks: highly crystalline graphite (which is usually formed at high temperatures) and α-carbyne (which is a natural carbon modification that has been previously found only among products of experiments). Other newly formed minerals of the geyserites are equilibrium chalcedony, talc, and tremolite. This suggests that the rocks were formed under conditions significantly different from those under which classic geyserites are produced. Geyserites in the Ol’khon area were most probably produced by silica-saturated solutions rich in certain ore components (Fe, Mn, Sb, As, and Y) and heated to temperatures of about 400°C. Travertine (dpeaa)DE-He213 Rift Zone (dpeaa)DE-He213 Siberian Craton (dpeaa)DE-He213 Siliceous Material (dpeaa)DE-He213 Chalcedony (dpeaa)DE-He213 Skovitina, T. M. aut Sklyarova, O. A. aut Kotov, A. B. aut Tolmacheva, E. V. aut Velikoslavinskii, S. D. aut Enthalten in Petrology Moscow : MAIK Nauka/Interperiodica Publ. [u.a.], 1996 22(2014), 6 vom: Nov., Seite 536-546 (DE-627)511882602 (DE-600)2235750-6 1556-2085 nnns volume:22 year:2014 number:6 month:11 pages:536-546 https://dx.doi.org/10.1134/S0869591114060046 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 22 2014 6 11 536-546
spelling	10.1134/S0869591114060046 doi (DE-627)SPR020203357 (SPR)S0869591114060046-e DE-627 ger DE-627 rakwb eng Sklyarov, E. V. verfasserin aut Late Quaternary high-temperature geyserites in the Ol’khon area, Baikal rift zone: Petrography, mineralogy, chemical composition, and genesis 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2014 Abstract Late Quaternary geyserites in the Ol’khon area, Baikal rift zone, are a geologically and petrologically unique rocks, which may provide information on the character of hydrothermal processes during the development of modern rift zones. The geyserites of this area are characterized by the presence of minerals atypical of such rocks: highly crystalline graphite (which is usually formed at high temperatures) and α-carbyne (which is a natural carbon modification that has been previously found only among products of experiments). Other newly formed minerals of the geyserites are equilibrium chalcedony, talc, and tremolite. This suggests that the rocks were formed under conditions significantly different from those under which classic geyserites are produced. Geyserites in the Ol’khon area were most probably produced by silica-saturated solutions rich in certain ore components (Fe, Mn, Sb, As, and Y) and heated to temperatures of about 400°C. Travertine (dpeaa)DE-He213 Rift Zone (dpeaa)DE-He213 Siberian Craton (dpeaa)DE-He213 Siliceous Material (dpeaa)DE-He213 Chalcedony (dpeaa)DE-He213 Skovitina, T. M. aut Sklyarova, O. A. aut Kotov, A. B. aut Tolmacheva, E. V. aut Velikoslavinskii, S. D. aut Enthalten in Petrology Moscow : MAIK Nauka/Interperiodica Publ. [u.a.], 1996 22(2014), 6 vom: Nov., Seite 536-546 (DE-627)511882602 (DE-600)2235750-6 1556-2085 nnns volume:22 year:2014 number:6 month:11 pages:536-546 https://dx.doi.org/10.1134/S0869591114060046 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 22 2014 6 11 536-546
allfields_unstemmed	10.1134/S0869591114060046 doi (DE-627)SPR020203357 (SPR)S0869591114060046-e DE-627 ger DE-627 rakwb eng Sklyarov, E. V. verfasserin aut Late Quaternary high-temperature geyserites in the Ol’khon area, Baikal rift zone: Petrography, mineralogy, chemical composition, and genesis 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2014 Abstract Late Quaternary geyserites in the Ol’khon area, Baikal rift zone, are a geologically and petrologically unique rocks, which may provide information on the character of hydrothermal processes during the development of modern rift zones. The geyserites of this area are characterized by the presence of minerals atypical of such rocks: highly crystalline graphite (which is usually formed at high temperatures) and α-carbyne (which is a natural carbon modification that has been previously found only among products of experiments). Other newly formed minerals of the geyserites are equilibrium chalcedony, talc, and tremolite. This suggests that the rocks were formed under conditions significantly different from those under which classic geyserites are produced. Geyserites in the Ol’khon area were most probably produced by silica-saturated solutions rich in certain ore components (Fe, Mn, Sb, As, and Y) and heated to temperatures of about 400°C. Travertine (dpeaa)DE-He213 Rift Zone (dpeaa)DE-He213 Siberian Craton (dpeaa)DE-He213 Siliceous Material (dpeaa)DE-He213 Chalcedony (dpeaa)DE-He213 Skovitina, T. M. aut Sklyarova, O. A. aut Kotov, A. B. aut Tolmacheva, E. V. aut Velikoslavinskii, S. D. aut Enthalten in Petrology Moscow : MAIK Nauka/Interperiodica Publ. [u.a.], 1996 22(2014), 6 vom: Nov., Seite 536-546 (DE-627)511882602 (DE-600)2235750-6 1556-2085 nnns volume:22 year:2014 number:6 month:11 pages:536-546 https://dx.doi.org/10.1134/S0869591114060046 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 22 2014 6 11 536-546
allfieldsGer	10.1134/S0869591114060046 doi (DE-627)SPR020203357 (SPR)S0869591114060046-e DE-627 ger DE-627 rakwb eng Sklyarov, E. V. verfasserin aut Late Quaternary high-temperature geyserites in the Ol’khon area, Baikal rift zone: Petrography, mineralogy, chemical composition, and genesis 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2014 Abstract Late Quaternary geyserites in the Ol’khon area, Baikal rift zone, are a geologically and petrologically unique rocks, which may provide information on the character of hydrothermal processes during the development of modern rift zones. The geyserites of this area are characterized by the presence of minerals atypical of such rocks: highly crystalline graphite (which is usually formed at high temperatures) and α-carbyne (which is a natural carbon modification that has been previously found only among products of experiments). Other newly formed minerals of the geyserites are equilibrium chalcedony, talc, and tremolite. This suggests that the rocks were formed under conditions significantly different from those under which classic geyserites are produced. Geyserites in the Ol’khon area were most probably produced by silica-saturated solutions rich in certain ore components (Fe, Mn, Sb, As, and Y) and heated to temperatures of about 400°C. Travertine (dpeaa)DE-He213 Rift Zone (dpeaa)DE-He213 Siberian Craton (dpeaa)DE-He213 Siliceous Material (dpeaa)DE-He213 Chalcedony (dpeaa)DE-He213 Skovitina, T. M. aut Sklyarova, O. A. aut Kotov, A. B. aut Tolmacheva, E. V. aut Velikoslavinskii, S. D. aut Enthalten in Petrology Moscow : MAIK Nauka/Interperiodica Publ. [u.a.], 1996 22(2014), 6 vom: Nov., Seite 536-546 (DE-627)511882602 (DE-600)2235750-6 1556-2085 nnns volume:22 year:2014 number:6 month:11 pages:536-546 https://dx.doi.org/10.1134/S0869591114060046 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 22 2014 6 11 536-546
allfieldsSound	10.1134/S0869591114060046 doi (DE-627)SPR020203357 (SPR)S0869591114060046-e DE-627 ger DE-627 rakwb eng Sklyarov, E. V. verfasserin aut Late Quaternary high-temperature geyserites in the Ol’khon area, Baikal rift zone: Petrography, mineralogy, chemical composition, and genesis 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2014 Abstract Late Quaternary geyserites in the Ol’khon area, Baikal rift zone, are a geologically and petrologically unique rocks, which may provide information on the character of hydrothermal processes during the development of modern rift zones. The geyserites of this area are characterized by the presence of minerals atypical of such rocks: highly crystalline graphite (which is usually formed at high temperatures) and α-carbyne (which is a natural carbon modification that has been previously found only among products of experiments). Other newly formed minerals of the geyserites are equilibrium chalcedony, talc, and tremolite. This suggests that the rocks were formed under conditions significantly different from those under which classic geyserites are produced. Geyserites in the Ol’khon area were most probably produced by silica-saturated solutions rich in certain ore components (Fe, Mn, Sb, As, and Y) and heated to temperatures of about 400°C. Travertine (dpeaa)DE-He213 Rift Zone (dpeaa)DE-He213 Siberian Craton (dpeaa)DE-He213 Siliceous Material (dpeaa)DE-He213 Chalcedony (dpeaa)DE-He213 Skovitina, T. M. aut Sklyarova, O. A. aut Kotov, A. B. aut Tolmacheva, E. V. aut Velikoslavinskii, S. D. aut Enthalten in Petrology Moscow : MAIK Nauka/Interperiodica Publ. [u.a.], 1996 22(2014), 6 vom: Nov., Seite 536-546 (DE-627)511882602 (DE-600)2235750-6 1556-2085 nnns volume:22 year:2014 number:6 month:11 pages:536-546 https://dx.doi.org/10.1134/S0869591114060046 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 22 2014 6 11 536-546
language	English
source	Enthalten in Petrology 22(2014), 6 vom: Nov., Seite 536-546 volume:22 year:2014 number:6 month:11 pages:536-546
sourceStr	Enthalten in Petrology 22(2014), 6 vom: Nov., Seite 536-546 volume:22 year:2014 number:6 month:11 pages:536-546
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Travertine Rift Zone Siberian Craton Siliceous Material Chalcedony
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container_title	Petrology
authorswithroles_txt_mv	Sklyarov, E. V. @@aut@@ Skovitina, T. M. @@aut@@ Sklyarova, O. A. @@aut@@ Kotov, A. B. @@aut@@ Tolmacheva, E. V. @@aut@@ Velikoslavinskii, S. D. @@aut@@
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author	Sklyarov, E. V.
spellingShingle	Sklyarov, E. V. misc Travertine misc Rift Zone misc Siberian Craton misc Siliceous Material misc Chalcedony Late Quaternary high-temperature geyserites in the Ol’khon area, Baikal rift zone: Petrography, mineralogy, chemical composition, and genesis
authorStr	Sklyarov, E. V.
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topic_title	Late Quaternary high-temperature geyserites in the Ol’khon area, Baikal rift zone: Petrography, mineralogy, chemical composition, and genesis Travertine (dpeaa)DE-He213 Rift Zone (dpeaa)DE-He213 Siberian Craton (dpeaa)DE-He213 Siliceous Material (dpeaa)DE-He213 Chalcedony (dpeaa)DE-He213
topic	misc Travertine misc Rift Zone misc Siberian Craton misc Siliceous Material misc Chalcedony
topic_unstemmed	misc Travertine misc Rift Zone misc Siberian Craton misc Siliceous Material misc Chalcedony
topic_browse	misc Travertine misc Rift Zone misc Siberian Craton misc Siliceous Material misc Chalcedony
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title	Late Quaternary high-temperature geyserites in the Ol’khon area, Baikal rift zone: Petrography, mineralogy, chemical composition, and genesis
ctrlnum	(DE-627)SPR020203357 (SPR)S0869591114060046-e
title_full	Late Quaternary high-temperature geyserites in the Ol’khon area, Baikal rift zone: Petrography, mineralogy, chemical composition, and genesis
author_sort	Sklyarov, E. V.
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author_browse	Sklyarov, E. V. Skovitina, T. M. Sklyarova, O. A. Kotov, A. B. Tolmacheva, E. V. Velikoslavinskii, S. D.
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title_sort	late quaternary high-temperature geyserites in the ol’khon area, baikal rift zone: petrography, mineralogy, chemical composition, and genesis
title_auth	Late Quaternary high-temperature geyserites in the Ol’khon area, Baikal rift zone: Petrography, mineralogy, chemical composition, and genesis
abstract	Abstract Late Quaternary geyserites in the Ol’khon area, Baikal rift zone, are a geologically and petrologically unique rocks, which may provide information on the character of hydrothermal processes during the development of modern rift zones. The geyserites of this area are characterized by the presence of minerals atypical of such rocks: highly crystalline graphite (which is usually formed at high temperatures) and α-carbyne (which is a natural carbon modification that has been previously found only among products of experiments). Other newly formed minerals of the geyserites are equilibrium chalcedony, talc, and tremolite. This suggests that the rocks were formed under conditions significantly different from those under which classic geyserites are produced. Geyserites in the Ol’khon area were most probably produced by silica-saturated solutions rich in certain ore components (Fe, Mn, Sb, As, and Y) and heated to temperatures of about 400°C. © Pleiades Publishing, Ltd. 2014
abstractGer	Abstract Late Quaternary geyserites in the Ol’khon area, Baikal rift zone, are a geologically and petrologically unique rocks, which may provide information on the character of hydrothermal processes during the development of modern rift zones. The geyserites of this area are characterized by the presence of minerals atypical of such rocks: highly crystalline graphite (which is usually formed at high temperatures) and α-carbyne (which is a natural carbon modification that has been previously found only among products of experiments). Other newly formed minerals of the geyserites are equilibrium chalcedony, talc, and tremolite. This suggests that the rocks were formed under conditions significantly different from those under which classic geyserites are produced. Geyserites in the Ol’khon area were most probably produced by silica-saturated solutions rich in certain ore components (Fe, Mn, Sb, As, and Y) and heated to temperatures of about 400°C. © Pleiades Publishing, Ltd. 2014
abstract_unstemmed	Abstract Late Quaternary geyserites in the Ol’khon area, Baikal rift zone, are a geologically and petrologically unique rocks, which may provide information on the character of hydrothermal processes during the development of modern rift zones. The geyserites of this area are characterized by the presence of minerals atypical of such rocks: highly crystalline graphite (which is usually formed at high temperatures) and α-carbyne (which is a natural carbon modification that has been previously found only among products of experiments). Other newly formed minerals of the geyserites are equilibrium chalcedony, talc, and tremolite. This suggests that the rocks were formed under conditions significantly different from those under which classic geyserites are produced. Geyserites in the Ol’khon area were most probably produced by silica-saturated solutions rich in certain ore components (Fe, Mn, Sb, As, and Y) and heated to temperatures of about 400°C. © Pleiades Publishing, Ltd. 2014
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container_issue	6
title_short	Late Quaternary high-temperature geyserites in the Ol’khon area, Baikal rift zone: Petrography, mineralogy, chemical composition, and genesis
url	https://dx.doi.org/10.1134/S0869591114060046
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author2	Skovitina, T. M. Sklyarova, O. A. Kotov, A. B. Tolmacheva, E. V. Velikoslavinskii, S. D.
author2Str	Skovitina, T. M. Sklyarova, O. A. Kotov, A. B. Tolmacheva, E. V. Velikoslavinskii, S. D.
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doi_str	10.1134/S0869591114060046
up_date	2024-07-03T14:33:06.244Z
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Late Quaternary high-temperature geyserites in the Ol’khon area, Baikal rift zone: Petrography, mineralogy, chemical composition, and genesis

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